Sunday, May 31, 2015

'Arctic methane skyrocketing' is the title of a video by Paul Beckwith discussing recent rises in methane levels in the Arctic.

Paul's description: "I discuss how ground level flask measurements of methane have been spiking upwards over the last few years. I analyze the implications to the breakdown of climate stability, causing jet stream fracturing and weather regime change. I believe that this behaviour will rapidly worsen as Arctic temperature amplification continues, leading our planet to a much warmer and unrecognizable climate over the next 5 to 10 years."

Thursday, May 28, 2015

On May 27, 2015, Arctic sea ice extent was merely 11.973 million square kilometers, a record low for the time of the year since satellite started measurements in 1979.

This fall in sea ice extent follows heat waves in Alaska and the north of Canada, as illustrated by the image below.

Temperature in Alaska on the afternoon of May 23, 2015, when a temperature of 91°F (32.78°C) was recorded in Eagle.

High temperatures extended over the Beaufort Sea and Chukchi Sea. The image below shows the difference in sea surface temperatures between May 13, 2015, and May 23, 2015.

The large amounts of meltwater flowing into Beaufort Sea and the Chukchi Sea is illustrated by the image below, showing the difference in sea surface salinity between May 17, 2015, and May 24, 2015.

Sea ice has retreated dramatically in the Chukchi Sea and the Beaufort Sea, and in Baffin Bay, with high sea surface temperature showing up where rivers flow into the Arctic Ocean and where the Gulf Stream carries warm water from the Atlantic Ocean into the Arctic Ocean.

The size-reduced navy.mil animations below show the fall in sea surface salinity (left) and the fall in sea ice thickness (right) in the Beaufort Sea, from May 3, 2015, to June 2, 2015 (run May 27, 2015).

High temperatures were reached at the city of Eagle, located on the southern bank of the Yukon River, at an elevation of 853 ft (260 m). High temperatures at such a location will cause meltwater, aggravating the situation well beyond the local area.

Carbon contained in soils will thus become increasingly exposed under the combined impact of rising temperatures and the associated growing amounts of meltwater. The meltwater can additionally cause erosion further downstream, thus making carbon at many locations become more prone to be consumed by microbes and released into the atmosphere in the form of carbon dioxide and methane.

This immense release would likely feed on itself, raising temperatures that continue melting more and more permafrost in a vicious, frightening, and unstoppable cycle. A tipping point could well be crossed, at which time human intervention is no longer possible. Temperatures across the planet could soar, setting in motion catastrophic levels of drought and food shortage. All life support systems on earth and life forms themselves could be placed under severe stress.

The colossal scale of the danger - and the observation of those factors lining up that could trigger it - demand that humanity exercise the precautionary principle. All political decision-making related to carbon emissions must be based on the understanding that a catastrophic consequence is looming, and the window of time for prevention quickly diminishing.

Thursday, May 21, 2015

On May 20, 2015, Arctic sea ice extent was only 12.425 million square km, a record low for the time of the year since satellite measurements began in 1979.

As the Arctic Sea Ice is at a historic low, Alaska faces temperatures as high as 31°C (87.8°F), as illustrated by the image below.

How is it possible for temperatures to get so high at locations so close to the North Pole?

Typhoon Dolphin

Dr. Michael Ventrice, Operational Scientist at The Weather Channel Professional Division points at two typhoons, Noul and Dolphin, that recently hit the western Pacific Ocean.

These typhoons do have some impact. Importantly, global warming is increasing the strength of cyclones. In other words, a greater impact of cyclones on the jet stream can be expected as a feedback of global warming.

Furthermore, global warming is directly changing the path followed by the North Polar Jet Stream, from a relatively straight path at a latitude of 60°N to a wildly meandering path that at some places merges with the Subtropical Jet Stream and reaching speeds as high as 267 km/h (166 mph) and that at other places moves high into the Arctic and reaches speeds as high as 170 km/h (106 mph).

On above image, part of the jet stream even moves right across the pole. Such changes to the jet stream constitute one out of numerous feedbacks of global warming, as discussed at the feedbacks page. Decline of the snow cover and sea ice in the Arctic is another such feedback.

As discussed in earlier posts, heat waves at high latitudes cause thawing of frozen soil and melting of glaciers and snow cover, This results in large amounts of water draining into rivers that end up in the Arctic Ocean. At the same time, heat waves also raise the temperature of the water in these rivers. The larger amounts of warmer water result in additional sea ice decline and warming of the Arctic Ocean seabed.

Such heat waves also set the scene for wildfires that emit not only greenhouse gases such as carbon dioxide and methane, but also pollutants such as carbon monoxide (that depletes hydroxyl that could otherwise break down methane) and black carbon (that when settling on ice causes it to absorb more sunlight).

Above image shows how much warmer the water in the Arctic Ocean is compared to what it used to be, with high anomalies where rivers flow into the Arctic Ocean and where the Gulf Stream carries warm water from the Atlantic Ocean into the Arctic Ocean.

The situation looks set to get worse, as the frequency and intensity of heat waves in North America and Siberia increases as temperature at high latitudes are rising rapidly. Furthermore, warm water is lining up along the path of the Gulf Stream, with sea surface temperature anomalies as high as 10.3°C (18.54°F) recorded off the coast of North America on May 20, 2015, as illustrated by the image below.

Friday, May 15, 2015

On May 12, 2015, a temperature of 80.1°F (or 26.7°C) was recorded in the north of Canada, at a location just north of latitude 63°N.

High temperatures in such locations are very worrying, for a number of reasons, including:

They are examples of heatwaves that can increasingly extend far to the north, all the way into the Arctic Ocean, speeding up warming of the Arctic Ocean seabed and threatening to unleash huge methane eruptions.

They set the scene for wildfires that emit not only greenhouse gases such as carbon dioxide and methane, but also pollutants such as carbon monoxide (that depletes hydroxyl that could otherwise break down methane) and black carbon (that when settling on ice causes it to absorb more sunlight).

They cause warming of the water of rivers that end up in the Arctic Ocean, thus resulting in additional sea ice decline and warming of the Arctic Ocean seabed.

The image below shows increased sea surface temperature anomalies in the area of the Beaufort Sea where the Mackenzie River is flowing into the Arctic Ocean.

The image below further illustrates the situation, with sea ice thickness (in m) down to zero where the Mackenzie River flows into the Arctic Ocean.

Things look set to get worse. The forecast for May 16, 2015, shows high temperatures extending all the way to the coast where the Mackenzie River flows into the Arctic Ocean.

Updates follow below:
Alaska is hit by high temperatures as well. The image below shows temperatures as high as 25.3°C (77.54°F) at a location just north of latitude 66°N in Alaska.

Below a forecast for May 23, 2015, showing temperatures in Alaska and neighboring parts of Canada that are 36°F (20°C) higher than they used to be (1979-2000 baseline).

The image below shows that temperatures as high as 30.2°C (86.36°F) are forecast for Alaska for May 23, 2015, along the path of the Yukon River, at a latitude of ~66 degrees North (65.98°N).

Furthermore, temperatures as high as 24.2°C (75.56°F) are forecast for the coast, close to where the Mackenzie River flows into the Arctic Ocean. Off the coast, over the water of the Arctic Ocean, temperatures as high as 8°C (46.4°F) are forecast, for a location just north of latitude 70°N, while temperatures as high as 15°C (59°F) are forecast for a location over the water of the Arctic Ocean closer to land.

As the image below illustrates, the jet stream is forecast to move across Alaska on May 23, 2015, bringing warm air into the atmosphere over the Arctic Ocean. The image gives the jet stream's speed at three locations, i.e. the jet stream is forecast to reach speeds as high as 262 km/h (162.8 mph, bottom green circle) over the Pacific Ocean, 165 km/h (102.5 mph, middle green circle) south of Alaska, and 172 km/h (106.9 mph, top green circle) over the Arctic Ocean.

Looking at salinity is a way to see the impact of rivers. The animation below, created with Naval Research Laboratory images over the period May 16 to 20, 2015 (run on May 18, 2015), shows salinity levels falling where the Mackenzie River flows into the Arctic Ocean.

Salinity works in several ways. Falling salinity will increase the temperature at which the sea ice melts. However, such an increase can only temporarily hold back melting, as illustrated by the combination image below, comparing sea ice thickness between May 7 and May 18, 2015.

Let's have a look at some of the feedbacks that haven't been discussed much in earlier posts. The potential for rivers to contribute to sea ice decline is depicted in the diagram below (feedback #24), i.e. extreme weather causing warming of rivers that flow into the Arctic Ocean. Furthermore, evaporation rates are higher over fresh water surfaces than over saline water surfaces (feedback #26) and the resulting increase in water vapor and clouds contributes to further warming (feedback #25), while rain falling on the sea ice will also cause its albedo to decline. The latter feedback also closes some loops. in that sea ice retreat results in more open water, in turn resulting in more water vapor and clouds.

Another feedback is that, as more sea ice turns into open water, less infrared radiation will be emitted and sent out into space, since open oceans are less efficient than sea ice when it comes to emitting in the far-infrared region of the spectrum (feedback #23). Furthermore, as sea ice declines, the increase in Arctic phytoplankton warms the ocean surface layer through direct biological heating (feedback #22).

For more discussion of these feedbacks, see the feedbacks page. In conclusion, the situation is dire and calls for comprehensive and effective action, as discussed at the Climate Plan page.

Forecast for May 16, 2015, showing high temperatures extending all the way to the coast where the Mackenzie River flows...
Posted by Sam Carana on Friday, May 15, 2015

Friday, May 8, 2015

For the first time since modern records began, monthly mean carbon dioxide levels were above 400 parts per million (ppm), as illustrated by the NOAA image below. NOAA just released the mean global carbon dioxide level for March 2015, which was 400.83 ppm.

Arctic Ocean hit hard

Carbon dioxide concentrations can be especially high, i.e. well over 410 ppm, at higher latitudes of the Northern Hemisphere, as illustrated by the NOAA image below. This can contribute to very high temperature anomalies over the Arctic Ocean and thus increase the risk of huge amounts of methane erupting from the Arctic Ocean seafloor.

Since the start of the Industrial Revolution, carbon dioxide levels have risen non-linearly, as illustrated by the image below.

Need for Comprehensive and Effective Action

As many posts at this blog have warned, emissions by people and the numerous feedbacks are threatening to push Earth into runaway global warming.

This calls for comprehensive and effective action to - among other things - reduce atmospheric carbon dioxide levels back to 280 ppm, as illustrated by the image below and as further discussed at the policies proposed as part of the Climate Plan.

How best to get back to 280 ppm?

The Climate Plan calls for restoration of greenhouse gas levels in oceans and atmosphere to their long term average by 2100. In the Climate Plan, multiple lines of action are proposed to work simultaneously, in parallel and separately in their implementation, yet complementary in their impact.
One line of action is to cut emissions by 80% by the year 2020. To achieve this, the Climate Plan advocates implementation of local feebates. Especially important are fees on sales of fuel, while the resulting revenues are best used to fund rebates on products sold locally that further help speed up the shift to clean energy.

Without further action, much of the carbon dioxide that has been emitted will stay in the atmosphere for hundreds, if not thousands of years. Therefore, further lines of action are needed, including removal of carbon dioxide from the atmosphere and oceans, with the carbon being safely stored.

For the long term average of 280 ppm to be achieved in 2100, large amounts of atmospheric carbon dioxide must also be removed and safely stored annually. How much must be removed? The period from 2015 to 2100 has 85 years, so bringing down carbon dioxide from 400 ppm to 280 ppm over that period works out to an annual removal of 1.41 ppm. By comparison, this is slightly less than the annual growth in carbon dioxide levels as caused by people since 1959, which is on average 1.47 ppm. Assuming that emissions will not be cut quickly enough to avoid further build up of carbon dioxide in the atmosphere in the near future, annual removal will need to be somewhat more, so 1.47 ppm looks like a good target for now, precisely because it equals past emissions.

The Climate Plan thus proposes that each nation will contribute to the necessary annual 1.47 ppm removal with a share that reflects its past emissions. The image below gives an idea of past emissions. Note that the image only shows emissions up to the year 2011 and that they exclude land use change and forestry emissions. Furthermore, the image shows emissions based on where products were produced. Much of the rise in emissions is the result of products that were produced in Asia, yet many of these products were consumed in Europe and North America. Therefore, graphs based on emissions where products were consumed would paint a somewhat different picture. The Climate Plan proposes that a nation's contributions to carbon dioxide removal (from oceans and atmosphere) will reflect its past emissions based on where products were consumed.

The Climate Plan advocates separate lines of action, i.e. greenhouse gas removal next to emission cuts and further action. Keeping action on different types of pollution separate and calling for local action in each nation further helps avoid that progress elsewhere is pointed at by a nation as an excuse to delay the necessary action on a specific type of pollution in that nation.

As said, the Climate Plan therefore calls for fees to be added on sales of polluting products where they are consumed (as opposed to where they are produced). Each nation is further expected to take steps to contribute its share to the 1.47 ppm carbon dioxide that needs to be removed from the atmosphere annually. Additionally, carbon dioxide needs to be removed from the oceans.

The most important thing each nation can do in the lead-up to the upcoming U.N. climate conference in Paris is to accept these commitments. How each nation and local community does achieve targets is best decided locally, provided that each nation and each local community does indeed reach its targets, and this follows from this commitment.

One reason why local feebates are recommended is that they can focus on achieving local targets for a specific pollutant. Local feebates allow communities to quickly adjust the height of the fees, where a local community threatens to fail reaching a target. Such a local focus does not preclude action being beneficial elsewhere as well. Indeed, the same feebate can work for multiple pollutants and on multiple lines of action. In this sense, locally implemented feebates often work complementary. As an example, the feebates pictured below will help remove carbon dioxide from the atmosphere and oceans, while they will also help cut emissions of carbon dioxide, methane, soot and nitrous oxide.

Videos

Global temperatures are rising fast. In the Arctic, temperatures are rising even faster (interactive charts below and right). For 2010 and 2011, NASA recorded anomalies of over 2°C at higher latitudes (64N to 90N), with anomalies of over 3°C at latitudes 79N and 81N in 2010.

For November 2010, anomalies of 12.5°C were recorded at latitude 71N, longitude -79 (Baffin Island, Canada). At specific moments in time and at specific locations, anomalies can be even more striking. As an example, on January 6, 2011, temperature in Coral Harbour, located at the northwest corner of Hudson Bay in the province of Nunavut, Canada, was 30°C (54°F) above average.